Articles | Volume 10, issue 2
Atmos. Chem. Phys., 10, 547–561, 2010
https://doi.org/10.5194/acp-10-547-2010
Atmos. Chem. Phys., 10, 547–561, 2010
https://doi.org/10.5194/acp-10-547-2010

  21 Jan 2010

21 Jan 2010

Carbonyl sulfide exchange in a temperate loblolly pine forest grown under ambient and elevated CO2

M. L. White et al.

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Subject: Biosphere Interactions | Research Activity: Field Measurements | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
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Cited articles

Aneja, V. P., Overton, J. H., Cupitt, L. T., Durham, J. L., and Wilson, W. E.: Carbon disulphide and carbonyl sulphide from biogenic sources and their contributions to the global sulphur cycle, Nature, 282, 493–496, 1979.
Barnes, I., Becker, K. H., and Patroescu, I.: The tropospheric oxidation of dimethyl sulfide: A new source of carbonyl sulfide, Geophys. Res. Lett., 21, 2389–2392, 1994.
Berresheim, H. and Vulcan, V. D.: Vertical distributions of COS, CS2, DMS and other sulfur compounds in a loblolly pine forest, Atmos. Environ., 26A, 2031–2036, 1992.
Bonan, G. B.: Forests and climate change: Forcings, feedbacks, and the climate benefits of forests, Science, 320, 1444, https://doi.org/10.1126/science.1155121, 2008.
Brown, K. A. and Bell, J. N. B.: Vegetation – the missing sink in the global cycle of carbonyl sulphide (COS), Atmos. Environ., 20, 537–540, 1986.
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